Based on water quality monitoring and numerical modeling, a conceptual model for turbidity generation in the Milandre Cave is proposed 10 • Turbidity peaks originating from soil erosion (allochthonous) and from karst sed-11 iment remobilization (autochthonous) have been distinguished 12 • The flooding and the emptying of epiphreatic conduits are pointed out as main 13 mechanisms for autochthonous turbidity generation
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